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Holocene paleoenvironmental reconstructions in western Brittany (Bay of Brest)

Part II – A 7 kyr human-environment story with a focus on the Neolithic-Bronze Age transition

Bibliographic Data

ID7170472
AuthorsClara Valero (0009-0009-2348-3686, Geo-Ocean, Univ Brest, Univ Bretagne Sud, CNRS, Ifremer, UMR6538, IUEM, F-29280 Plouzané, France, corresponding author), Aurélie Penaud (0000-0003-3578-4549, Geo-Ocean, Univ Brest, Univ Bretagne Sud, CNRS, Ifremer, UMR6538, IUEM, F-29280 Plouzané, France), Clément Lambert (0000-0002-7746-8504, Geo-Ocean, Univ Bretagne Sud, Univ Brest, CNRS, Ifremer, UMR6538, F-56000 Vannes, France), Muriel Vidal (0000-0003-3699-2083, Geo-Ocean, Univ Brest, Univ Bretagne Sud, CNRS, Ifremer, UMR6538, IUEM, F-29280 Plouzané, France), Yvan Pailler (0000-0002-4782-1389, Geo-Ocean, Univ Bretagne Sud, Univ Brest, CNRS, Ifremer, UMR6538, F-56000 Vannes, France), Clément Nicolas (0000-0003-3258-4920, Laboratoire Trajectoires, CNRS, Université Paris 1 - Panthéon Sorbonne, UMR8215, F-75105 Paris Cedex 05, France), Olivier Poncin (CRBC - Centre de Recherche Bretonne et Celtique, Univ Brest, UR4451, F-29200 Brest, France), Pierre Stéphan (0000-0001-7975-2149, Univ Brest, Univ Nantes, Univ Rennes, CNRS, LETG UMR6554, IUEM, F-29280 Plouzané, France), Axel Ehrhold (0000-0001-7207-0831, Geo-Ocean, Univ Brest, Univ Bretagne Sud, CNRS, Ifremer, UMR6538, IUEM, F-29280 Plouzané, France)
Year2025
Volume35
Issue5
Pages541-555
Publication date2025-05-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publications Inc (PUBLISHER)
DOI10.1177/09596836251313635
OpenAlexW4406954578
LanguageEN
References cited74

The Bay of Brest (BB, NW France) is a semi-enclosed basin of 180 km2 subject to macro-tidal dynamics and to the fluvial influences of the rivers Aulne and Elorn, which combined drain watersheds of 2600 km2. This coastal environment is subject to natural climate oscillations overlaid on the long-term landscape transformations inherited from the post-glacial sea level rise and increasing anthropogenic forcing since the Neolithic (6.9 ka BP), and especially from the Bronze Age (4.2 ka BP) onwards. The BB therefore appears suitable for the reconstruction of the interactions between climate, environment and human dynamics across the Holocene. In this study, a palynological stack was created based on five cores (including two new cores PALM-KS05 and PALM-KS06 from the Brest harbour), allowing us to discuss vegetation dynamics over the last 7 kyrs. Since the Neolithic period, the forest cover has decreased in favour of open and agro-pastoral landscapes. This trend is not uniform, however: forest cover first declined slowly around 4 ka BP, then strongly decreased at the end of the Iron Age, before experiencing a revival of about five centuries at the end of the Roman period (1.7–1.2 ka BP). Finally, a drastic fall of tree pollen taxa is recorded at the start of the Middle Ages. This study is the first on long-term Holocene trends that allows discussion of both climatic and anthropogenic forcing at an unprecedent average study resolution of 35 years. We also place this local evolution in a wider context to detail interactions between natural and anthropic forcings over the last 7 kyrs BP at a regional-scale and we discuss paleoenvironments and human dynamics thanks to the incorporation of an up-to-date corpus of archaeological data

Archaeology · Bay · Bronze Age · Fluvial · Geography · Holocene · Holocene climatic optimum · Palynology · Physical geography · Pollen · Sea level · Shore · Structural basin · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Maritime and Coastal Archaeology · Ecology · Geology · Oceanography · Paleontology

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Citation velocityhistorical
Highly citedNo
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